The Caucasus is the highest mountains in Russia. Famous mountains of Russia and their height

Greater Caucasus- a mountain system between the Black and Caspian Seas. It extends for more than 1100 km from the northwest to the southeast, from the Anapa region and the Taman Peninsula to the Absheron Peninsula on the Caspian coast, near Baku. The highest peak is Elbrus (5642 m).

The state border of the Russian Federation with Abkhazia, Georgia, South Ossetia and Azerbaijan passes through the Greater Caucasus.

Scheme of the ridges of the Greater Caucasus. Volcanoes are marked with red circles.

The Greater Caucasus, together with the Lesser Caucasus, makes up the Caucasus Mountains and is separated from the latter by the Colchis and Kura-Araks lowlands and the Kura valley in the middle reaches between them.

The Greater Caucasus reaches its maximum width in the Elbrus region (up to 180 km). In the axial part is located the Main Caucasian (or Dividing) Range, to the north of which a number of parallel ranges (mountain ranges) extend - the Side Range, the Rocky Range, etc.

Parts and districts

View from Ushba to Elbrus. Photo by O. Fomichev.

Traditionally, the Greater Caucasus is divided into 3 parts:

Table 1. The peaks of the Caucasus are higher than 4700 m (bold font indicates the height according to the topographic map at a scale of 1:50000).

Climate

Rest in the Adish Icefall. Photo by A. Lebedev (1989)

The climatic features of the Greater Caucasus are determined by the altitudinal zonality and the rotation of the mountain barrier formed by it at a certain angle to the western moisture-bearing air flows - the Atlantic cyclones and the Mediterranean western air currents of the middle layers of the troposphere. This rotation has a decisive influence on the distribution of precipitation.

The wettest is the western part of the southern slope, where more than 2500 mm of precipitation falls annually in the highlands. The record amount of precipitation falls on the Achishkho ridge near Krasnaya Polyana - 3200 mm per year, this is the wettest place in Russia. Winter snow cover in the area of ​​the meteorological station Achishkho reaches 5-7 meters!

Glaciation is especially significant in the Central Caucasus and in the eastern part of the Western Caucasus. In the Eastern Caucasus, small glaciers are found only in individual high mountain nodes.

Caucasian mountains- the great division between Europe and Asia. The Caucasus is a narrow strip of land between the Black and Caspian Seas. It strikes with an incredible variety of climate, flora and fauna.

The pride of the Caucasus is its mountains! The Caucasus is not the Caucasus without mountains. The mountains are unique, majestic and impregnable. The Caucasus is amazingly beautiful. He is so different. You can look at the mountains for hours.

The mountain range of the Greater Caucasus is a lot of pastures, forests, as well as amazing natural wonders. More than 2 thousand glaciers descend through narrow gorges. The chain of large mountains stretched for almost one and a half thousand kilometers from the northwest to the southeast. The main peaks exceed 5 thousand meters and significantly affect the weather in the regions. The clouds that form over the Black Sea are pouring rain, running into the mountain peaks of the Caucasus. On one side of the ridge there is a harsh landscape, and on the other - rough vegetation. Here you can find more than 6 and a half thousand plant species, a quarter of which cannot be found anywhere else in the world.

There are many legends about the origin of the Caucasus Mountains:

A long time ago, when the earth was still very young, a huge plain stretched on the site of the modern territory of the Caucasus. Huge sled heroes lived here in peace and love. They were kind and prudent, they met with joy both day and night, they knew neither evil, nor envy, nor deceit. The ruler of this people was the gray-haired giant Elbrus, and he had a beautiful son, Beshtau, and his son had a charming bride, the beautiful Mashuki. But they had an evil envious - Kite. And he decided to harm the Narts. He prepared a terrible potion in which he mixed the teeth of a wolf, the tongue of a boar and the eyes of a snake. At a big feast, he poured a potion into all the drinks of the Narts. And, having drunk it, they acquired the greed of a boar, the anger of a wolf, and the deceit of a snake. And from that time on, the happy and carefree life of the Narts ended. The father decided to take the young bride away from his son and, sending him on a hunt, wanted to forcefully marry Mashuki. But Mashuki resisted Elbrus. And in an evil battle she lost her wedding ring. I saw the Beshtau ring and hurried to help the bride. And a terrible battle began not for life, but for death, and half of the Narts fought on the side of Elbrus, and the other half on the side of Beshtau. And the battle lasted for several days and nights, and all the sledges perished. Elbrus chopped his son into five parts, and the son, inflicting the last blow, dismembered the gray head of his father into two halves. Mashuki came out after the battle on the battlefield and did not see a single living soul. She approached her lover and plunged the dagger into her heart. So the life of a great and old people stopped.

And now the Caucasian mountains rise in this place: the helmet from the head of Beshtau is Mount Zheleznaya, the Mashuk ring is Mount Koltso, five peaks are Mount Beshtau, nearby is Mount Mashuk and far, far from the others - gray-haired or simply snow-covered handsome Elbrus.

The Caucasus Mountains are the result of the convergence of two plates

Let's look at one of the narrowest places in this grandiose mountain belt. At its northern outskirts, in Ciscaucasia, there are flat areas that belong to a solid plate called the Scythian. Further to the south are the sublatitudinal (that is, stretching approximately from west to east) mountains of the Greater Caucasus up to 5 km high, the narrow depressions of Transcaucasia - the Rionskaya and Kura lowlands - and also the sublatitudinal, but convex to the north mountain ranges of the Lesser Caucasus in Georgia, Armenia , Eastern Turkey and Western Iran (up to 5 km high).

To the south are the plains of Northern Arabia, which, like the plains of Ciscaucasia, belong to a very strong, monolithic Arabian lithospheric plate.

Therefore, the Scythian and Arabian plates- it's like two parts of a giant vise, which are slowly approaching, crushing everything that is between them. It is curious that directly opposite the northern, relatively narrow end of the Arabian Plate, in Eastern Turkey and Western Iran, there are the highest mountains in comparison with the mountains located to the west and east. They rise just in the place where the Arabian plate, like some kind of solid wedge, squeezed the pliable deposits most strongly.

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The Achishkho mountain range is the closest range to Krasnaya Polyana and the most picturesque. The highest mountain - Achishkho has a height of 2391 meters above sea level. An interesting fact about the name of the ridge: "Achishkho" in translation from the Abkhazian means "horse". This confirms the view from below, from Polyana to the mountain range. If you look closely, you can see the outline of a horse. The most popular hiking route passes through a special place located on the side of the mountain, approximately 1800 meters above sea level, where there was a weather station from the 30s to the 90s.

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The Aibga mountain range is located on the territory of the Sochi National Park, on the eastern side of Krasnaya Polyana. The ridge has a length of more than 20 kilometers, and consists of four highest points, called peaks. The most popular mountain peak among tourists is the Black Pyramid, 2375 meters above sea level. It has an unusual shape, which is why it is especially popular with climbers. In addition, a wonderful, breathtaking landscape opens up from the top of the mountain. Having conquered this mountain, you will see the valley of the Mzymta River, the peaks of Chugush and Pseashkho.

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One of the most beautiful resort places in our country is Dombay. The main attractions of this city are its scenic spots. Mussa Ridge - Achitara is considered the most picturesque ridge of this part of the Caucasus. In order to appreciate all the beauty surrounding the guests of the resort, you need to climb the mountainside by cable car. This place offers a wonderful picturesque view of the peaks and glaciers of the Main Range, the Teberda and Gonachkhiri valleys.

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Peak Ine is located near the place where the northern Dzhugurlutchat glacier originates. The name of the mountain is translated as "Needle", the mountain got its name because of its pointed top, this unusual view of mountains attracts many tourists from all over the world. The top of Ine Peak is covered with snow all year round, and although its sheer cliffs are relatively difficult to conquer, the top of Ine Peak is quite a popular destination for climbers. The height of the "needle" reaches 3455 meters, which is about 600 meters below the highest mountain of the Caucasus Dividing Range. It is best to view the mountain from the site of Mount Mussa-Achi-Tara, it is 400 meters lower than Ine Peak, but for that it can be reached by funicular.

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In the North Caucasus, among the Dombai glade, somewhat east of the mountain of the Back (Small) Belalakai, a peak called Sufruju spread out. The height of the mountain is 3871 m. A wide depression divides the massif into two equal parts - Southern and Northern. Both peaks are clearly visible from the ski Musat-Cheri. The southern part was called Sufruju's Tooth, which means "Tiger's Fang". The massif stretches for 3600 m and acts as the main attraction of the mountain Dombai.

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Belalakai is a mountain located near the village in Dombay, since the village is a resort mountain has become a symbol of this village and attracts a lot of tourists. Its height is 3861 meters. Although the height of this mountain is 200 meters lower than the highest in Abkhazia, it is no less an attraction. Belalakai owes its fame to quartz. Most of the mountain consists of dark rocks of soil and dark granite, however, due to centuries of geological processes, there are deposits of quartz on the mountain. It is this quartz that has created the white streaks that adorn the top of this mountain, the white streaks of Belalakai are especially visible at the end of summer. Because of the beauty of the local landscapes, the mountain was mentioned more than once in songs and poems.

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Dzhuguturluchat is a relatively small massif, in the large Caucasian ridge. In height, the mountain range rose to 3921 meters, which is only 120 meters less than the highest point on the Caucasus Range. Herds of tours are found in the highest regions of the mountain range, it was they who gave these mountains the name "Dzhugurluchat" - which translates as: "herd of tours". The mountain range originates from the Dombay plateau, however, the most beautiful places open from a place called "Mussa-Achi-Tara" where most tourists gather.

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Cheget is one of the highest mountains in the Caucasus. Its height reaches about 3770 meters. It is a popular tourism destination among travelers. From the mountain you can enjoy the view of the highest peak in Europe - Elbrus. Another feature of Mount Cheget is the second line of the cable car, which passes through the area where the snow lies, which does not melt throughout the year.There are three lines of the cable car in total. The height of the first reaches about 1600 meters. It is one of the most popular for tourists who come to Cheget to enjoy the view of Elbrus.

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This mountain after Elbrus is the second most popular among climbers. All because it is also quite high - 4454 meters above sea level.

There are several ways to get to the mountain by cable car or on foot. Tourists who have chosen the first method can use the Cheget cable car at the final point, where small cafes are located. The second and more difficult path, which takes several hours, is from the Cheget glade along a path already full of tourists. However, it is better to go on a journey with an experienced guide, otherwise there is a chance to get lost in the mountains.

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The North Caucasus will captivate many tourists with its beauties and landscapes. Mount Semyonov-Bashi, located in the east of the Caucasus Range, is no exception. In reality, this is just a ledge 3602 m above the ground. The mountain was named after the Russian explorer P.P. Semenov-Tyan-Shansky. This person was a traveler and was the chairman of the Russian Geographical Society.

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Mount Chotcha is part of the Caucasian ridge, which is famous for its picturesque mountains and rocks. Chotcha, unlike other mountains, is divided into two parts, as if someone cut the mountain in the middle into two halves. Unlike the mountains, which have just a smaller mountain nearby, at first glance it is clear that the mountain has one base on which there are two rocks. The rock in the foreground is lower than the back one, it has 3637 meters in height, it is 400 meters lower than the highest mountain of the Caucasian ridge. The second rock is only three meters higher than the first one, it is 3640 meters above sea level.

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Mount Ertsog is included in the list of one of the most visited places of the Caucasian ridge. At the foot of the mountain, the Alibek River flows, in addition to the mountain itself, this place has a very beautiful lowland. In the gorge where the river flows, a massive slope descends, it becomes especially beautiful in spring, when the sun illuminates the slope full of bright green vegetation. Mount Ertsog is part of the Teberdinsky ridge, the ridge itself encircles a lowland with a river and makes a very strong impression on tourists who visit it.

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Mount Sulohat is located in the Dombay region and is one of the largest points of the Caucasian watershed. The height of the mountain is 3439 meters, which is about 600 meters lower than the largest mountain on the Caucasian ridge. Mount Sulohat is surrounded by many legends, the most popular one is about the origin of the name of the mountain. In ancient times, the Alans tribe inhabited the foot of the mountain. In this tribe lived a girl named Sulohat, she was of extraordinary beauty and courage and was the daughter of the leader of the tribe.

Geographical position. On a huge isthmus between the Black and Caspian Seas, from the Taman Peninsula to the Apsheron Peninsula, the majestic mountains of the Greater Caucasus are located.

North Caucasus- this is the southernmost part of the Russian territory. The border of the Russian Federation with the countries of Transcaucasia runs along the ridges of the Main, or Dividing, Caucasian Range.

The Caucasus is separated from the Russian Plain by the Kuma-Manych depression, on the site of which a sea strait existed in the Middle Quaternary.

The North Caucasus is an area located on the border of the temperate and subtropical zones.

The epithet "most-most" is often applied to the nature of this territory. Latitudinal zonality is replaced here by vertical zonality. For an inhabitant of the plains, the mountains of the Caucasus are a vivid example of the “multi-story ™” of nature.

Remember where and what is the name of the extreme southern point of Russia.

Features of the nature of the North Caucasus. The Caucasus is a young mountain structure, formed during the period of Alpine folding. The Caucasus includes: Ciscaucasia, Greater Caucasus and Transcaucasia. Only Ciscaucasia and the northern slopes of the Greater Caucasus belong to Russia.

Rice. 92. Orographic scheme of the Caucasus

Often the Greater Caucasus is presented as a single ridge. In fact, it is a system of mountain ranges. From the Black Sea coast to Mount Elbrus is the Western Caucasus, from Elbrus to Kazbek - the Central Caucasus, east of Kazbek to the Caspian Sea - the Eastern Caucasus. In the longitudinal direction, an axial zone is distinguished, occupied by the Vodorazdelny (Main) and Lateral ridges.

The northern slopes of the Greater Caucasus form the Skalisty and Pastbishny ranges. They have a cuesta structure - these are ridges, in which one slope is gentle, and the other is abruptly ending. The reason for the formation of kuest is the interbedding of layers composed of rocks of different hardness.

The chains of the Western Caucasus begin near the Taman Peninsula. At first, these are not even mountains, but hills with soft outlines. They rise as you move east. Mountains Fisht (2867 m) and Oshten (2808 m) - the highest parts of the Western Caucasus - are covered with snowfields and glaciers.

The highest and most grandiose part of the entire mountain system is the Central Caucasus. Here, even the passes reach a height of 3000 m, only one pass - Krestovy on the Georgian Military Highway - lies at an altitude of 2379 m.

In the Central Caucasus there are the highest peaks - the two-headed Elbrus, an extinct volcano, the highest peak in Russia (5642 m), and Kazbek (5033 m).

The eastern part of the Greater Caucasus is mainly the numerous ridges of the mountainous Dagestan (in translation - the Country of Mountains).

Rice. 93. Mount Elbrus

Various tectonic structures took part in the structure of the North Caucasus. In the south there are folded-block mountains and foothills of the Greater Caucasus. It is part of the Alpine geosynclinal zone.

The fluctuations of the earth's crust were accompanied by bending of the earth's layers, their extensions, faults, ruptures. Magma poured out to the surface along the cracks formed from great depths, which led to the formation of numerous ore deposits.

Uplifts in recent geological periods - Neogene and Quaternary - have turned the Greater Caucasus into a mountainous country. The rise in the axial part of the Greater Caucasus was accompanied by an intensive subsidence of earth layers along the edges of the emerging mountain range. This led to the formation of foothill troughs: in the west of the Indolo-Kuban and in the east of the Terek-Caspian.

The complex history of the geological development of the region is the reason for the richness of the bowels of the Caucasus in various minerals. The main wealth of Ciscaucasia is the oil and gas field. Polymetallic ores, tungsten, copper, mercury, and molybdenum are mined in the central part of the Greater Caucasus.

In the mountains and foothills of the North Caucasus, many mineral springs have been discovered, near which resorts have been created that have long gained worldwide fame - Kislovodsk, Mineralnye Vody, Pyatigorsk, Essentuki, Zheleznovodsk, Matsesta. The springs are diverse in chemical composition, in temperature, and extremely useful.

Rice. 94. Geological structure of the North Caucasus

The geographical position of the North Caucasus in the south of the temperate zone determines its mild, warm climate, transitional from temperate to subtropical. Here is a parallel 45 ° N. sh., that is, this territory is equidistant from both the equator and the pole. This situation determines the amount of solar heat received: in summer 17-18 kcal per square centimeter, which is 1.5 times more than the European part of Russia receives on average. With the exception of the highlands, the climate in the North Caucasus is mild and warm; on the plains, the average temperature in July exceeds 20 ° C everywhere, and summer lasts from 4.5 to 5.5 months. Average January temperatures range from -10 to +6°C, and winter lasts only two to three months. The city of Sochi is located in the North Caucasus, where the warmest winter in Russia is with a January temperature of +6.1 ° С.

On the map, determine whether there are any obstacles in the foothills of the North Caucasus in the way of arctic air masses, tropical. What atmospheric fronts pass near this area? Analyze on maps how precipitation is distributed in the North Caucasus, explain the reasons for this distribution.

The abundance of heat and light allows the vegetation of the North Caucasus to develop in the north of the region for seven months, in Ciscaucasia - eight, and on the Black Sea coast, south of Gelendzhik - up to 11 months. This means that with the appropriate selection of crops, two crops per year can be obtained here.

The North Caucasus is distinguished by a very complex circulation of various air masses. Various air masses can penetrate into this area.

The main source of moisture for the North Caucasus is the Atlantic Ocean. Therefore, the western regions of the North Caucasus are characterized by a large amount of precipitation. The annual amount of precipitation in the foothill areas in the west is 380-520 mm, and in the east, in the Caspian Sea, - 220-250 mm. Therefore, in the east of the region there are often droughts and dry winds. However, they are often accompanied by dusty, or black, storms. Storms occur in the spring, when the top layers of dry soil, still loosely held together by newly emerged plants, are blown away by strong winds. A cloud of dust rises into the air, covering the sky and the sun.

Measures to combat black storms are properly planned forest shelterbelts and high agricultural technology. However, until now, due to black storms, it is necessary to re-sow (re-sow) several tens of thousands of hectares, from which the most fertile soil layer is demolished during dust storms.

The climate of the highlands very different from the plains and foothills. The first main difference is that much more precipitation falls in the mountains: at an altitude of 2000 m - 2500-2600 mm per year. This is due to the fact that the mountains trap air masses, forcing them to rise up. At the same time, the air cools and gives off its moisture.

The second difference in the climate of the highlands is a decrease in the duration of the warm season due to a decrease in air temperature with height. Already at an altitude of 2700 m on the northern slopes and at an altitude of 3800 m in the Central Caucasus there is a snow line, or the border of "eternal ice". At an altitude of over 4000 m, even in July, positive temperatures are very rare.

Remember how much the air temperature decreases when you rise for every 100 m. Calculate how much the air will cool when you rise to a height of 4000 m, if its temperature at the earth's surface is +20 ° С. What happens to the moisture in the air?

In the mountains of the Western Caucasus, due to the abundance of precipitation during the winter, a four-five-meter layer of snow accumulates, and in the mountain valleys, where it is blown away by the wind, up to 10-12 m. The abundance of snow in winter leads to the formation of snow avalanches. Sometimes one awkward movement, even a sharp sound, is enough for a thousand-ton mass of snow to fly down a steep ledge, destroying everything in its path.

Explain why there are practically no avalanches in the mountains of the Eastern Caucasus.

Think about what differences will be observed in the change of altitudinal zones on the western and eastern slopes.

The third difference of the alpine climate is its amazing diversity from place to place in connection with the height of the mountains, the exposure of the slope, proximity or distance from the sea.

The fourth difference is the peculiarity of atmospheric circulation. Cooled air from the highlands rushes down the comparatively narrow intermountain valleys. For every 100 m lowered, the air heats up by about 1°C. Descending from a height of 2500 m, it heats up by 25 ° C and becomes warm, even hot. This is how the local wind - foehn is formed. Hair dryers are especially frequent in spring, when the intensity of the general circulation of air masses increases sharply. Unlike a foehn, when masses of dense cold air invade, a bora is formed (from the Greek boreas - north, north wind), a strong cold downward wind. Flowing over low ridges into an area with warmer rarefied air, it heats up relatively little and “falls” down the leeward slope at high speed. Bora is observed mainly in winter, where the mountain range borders on the sea or a vast body of water. The Novorossiysk Bora is widely known (Fig. 95). And yet, the leading factor in climate formation in the mountains, which greatly affects all other components of nature, is the height, which leads to vertical zonality of both climate and natural zones.

Rice. 95. Scheme of formation of the Novorossiysk bora

The rivers of the North Caucasus are numerous and, like the relief and climate, are clearly divided into flat and mountainous. Stormy mountain rivers are especially numerous, the main source of food for which is snow and glaciers during the melting period. The largest rivers are the Kuban and the Terek with their numerous tributaries, as well as the Bolshoy Egorlyk and Kalaus, which originate in the Stavropol Upland. In the lower reaches of the Kuban and the Terek there are floodplains - vast swampy areas covered with reeds and reeds.

Rice. 96. Altitudinal zonality of the Greater Caucasus

The wealth of the Caucasus is fertile soil. In the western part of Ciscaucasia, chernozems predominate, and in the eastern, more arid part, chestnut soils. The soils of the Black Sea coast are intensively used for orchards, berry fields, and vineyards. The northernmost tea plantations in the world are located in the Sochi region.

In the mountains of the Greater Caucasus, altitudinal zonation is clearly expressed. The lower belt is occupied by broad-leaved forests dominated by oak. Above are beech forests, which with height pass first into mixed, and then into spruce-fir forests. The upper border of the forest is located at an altitude of 2000-2200 m. Behind it, on mountain-meadow soils, there are lush subalpine meadows with thickets of Caucasian rhododendron. They pass into short-grass alpine meadows, followed by the highest belt of snowfields and glaciers.

Questions and tasks

1. On the example of the North Caucasus, show the influence of the geographical location of the territory on the features of its nature.
2. Tell us about the formation of the modern relief of the Greater Caucasus.
3. On the contour map, mark the main geographical features of the area, mineral deposits.
4. Give a description of the climate of the Greater Caucasus, explain how the climate of the foothills differs from the highlands.

Surprisingly beautiful mountain landscapes can be seen in these wonderful and unique places. The most impressive peaks are the Greater Caucasus Range. This is the territory of the highest and largest mountains in the Caucasus region.

The Lesser Caucasus and the valleys (Riono-Kura depression) represent Transcaucasia in the complex.

Caucasus: general description

The Caucasus is located between the Caspian Sea and the Black Sea in southwestern Asia.

This region includes the mountains of the Greater and Lesser Caucasus, as well as the depression between them called the Riono-Kura depression, the coasts of the Black Sea and the Caspian Seas, the Stavropol Upland, a small part of the Caspian lowland (Dagestan) and the Kuban-Azov lowland to the left bank of the Don River on part of its mouth.

The mountains of the Greater Caucasus have a length of 1500 kilometers, and the highest peak is Elbrus. The length of the Lesser Caucasus Mountains is 750 km.

A little lower, let's take a closer look at the Caucasus Range.

Geographical position

In the western part, the Caucasus borders on the Black and Azov seas, in the east - on the Caspian. In the north, the East European Plain extends, and the border between it and the Caucasian foothills repeats the latter passes along the river. Kuma, the bottom of the Kumo-Manychskaya depression, along the Manych and Vostochny Manych rivers, and then along the left bank of the Don.

The southern border of the Caucasus is the Araks River, behind which are the Armenian and Iranian Highlands, and the river. Chorokh. And already beyond the river, the peninsulas of Asia Minor begin.

Caucasian Range: description

The most courageous people and climbers have long chosen the Caucasian mountain range, which attracts extreme people from all over the world.

The most important Caucasian ridge divides the entire Caucasus into 2 parts: Transcaucasia and the North Caucasus. This mountain range extends from the Black Sea to the shores of the Caspian Sea.

The length of the Caucasus Range is more than 1200 kilometers.

The site, located on the territory of the reserve, represents the highest mountain ranges of the Western Caucasus. Moreover, the heights here are the most diverse. Their marks vary from 260 to more than 3360 meters above sea level.

The perfect combination of mild mild climate and amazing landscapes make this place ideal for an active tourist holiday at any time of the year.

The main Caucasian ridge in the Sochi territory has the largest peaks: Fisht, Khuko, Lysaya, Venets, Grachev, Pseashkho, Chugush, Malaya Chura and Assara.

The composition of the rocks of the ridge: limestones and marls. There used to be an ocean floor here. Throughout the vast massif, one can observe a pronounced folding with numerous glaciers, turbulent rivers and mountain lakes.

About the height of the Caucasus Range

The peaks of the Caucasus Range are numerous and quite diverse in height.

Elbrus is the highest point of the Caucasus, which is the highest peak not only in Russia, but also in Europe. The location of the mountain is such that a variety of nationalities live around it, giving it their unique names: Oshkhomakho, Alberis, Yalbuz and Mingitau.

The most important mountain in the Caucasus ranks fifth on Earth among mountains formed in this way (as a result of a volcanic eruption).

The height of the most gigantic peak in Russia is five kilometers six hundred and forty-two meters.

More details about the highest peak of the Caucasus

The highest height of the Caucasus Range is Russia. It looks like two cones, between which (a distance of 3 km from each other) at an altitude of 5200 meters there is a saddle. The highest of them has, as already noted, a height of 5642 meters, a smaller one - 5621m.

Like all peaks of volcanic origin, Elbrus consists of 2 parts: a 700-meter pedestal of rocks and a bulk cone (1942 meters) - the result of a volcanic eruption.

The peak is covered with snow starting from a height of about 3500 meters. In addition, there are glaciers, the most famous of which are the Small and Big Azau and Terskop.

The temperature at the highest point of Elbrus is -14 °C. Precipitation here almost always falls in the form of snow and therefore the glaciers do not melt. Due to the good visibility of the Elbrus peaks from different remote places and at different times of the year, this mountain also has an interesting name - Small Antarctica.

It should be noted that for the first time the eastern peak was conquered by climbers in 1829, and the western one - in 1874.

Glaciers located on the top of Elbrus feed the Kuban, Malka and Baksan rivers.

Central Caucasus: ridges, parameters

Geographically, the Central Caucasus is part of the Greater Caucasus, located between the mountains of Elbrus and Kazbek (in the west and in the east). In this section, the length of the Main Caucasian Range is 190 kilometers, and if we take into account the meanders, about 260 km.

The border of the Russian state passes through the territory of the Central Caucasus. Behind it are South Ossetia and Georgia.

22 kilometers west of Kazbek (eastern part of the Central Caucasus), the Russian border shifts slightly to the north and runs to Kazbek, skirting the Georgian-owned Terek River valley (upper part).

On the territory of the Central Caucasus, 5 parallel ridges are distinguished (oriented along the latitudes):

1. The main Caucasian ridge (height up to 5203 m, Mount Shkhara).
2. Ridge Lateral (height up to 5642 meters, Mount Elbrus).
3. Ridge Rocky (height up to 3646 meters, Mount Karakaya).
4. Ridge Pastbishchny (up to 1541 meters).
5. Ridge Wooded (height 900 meters).

Tourists and climbers mainly visit and storm the first three ridges.

North and South Caucasus

The Greater Caucasus, as a geographical object, originates from the Taman Peninsula, and ends in the region. All subjects of the Russian Federation and countries located in this region belong to the Caucasus. However, in terms of the location of the territories of the constituent entities of Russia, there is a certain division into two parts:

• The North Caucasus includes the Krasnodar Territory and Stavropol Territory, North Ossetia, the Rostov Region, Chechnya, the Republic of Adygea, Ingushetia, Kabardino-Balkaria, Dagestan and Karachay-Cherkessia.
• South Caucasus (or Transcaucasia) - Armenia, Georgia, Azerbaijan.

Elbrus region

The Elbrus region is geographically the westernmost section of the Central Caucasus. Its territory covers the upper reaches of the Baksan River with its tributaries, the area north of Elbrus and the western spurs of Mount Elbrus to the right bank of the Kuban. The largest peak of this region is the famous Elbrus, located to the north and located in the Side Range. The second highest peak is (4700 meters).

The Elbrus area is famous for a large number of peaks with steep ridges and rocky walls.

The largest glaciers are concentrated in the huge Elbrus glacier complex, which has 23 glaciers (total area - 122.6 sq. km).

Location of states in the Caucasus

1. The Russian Federation partially occupies the territory of the Greater Caucasus and its foothills from the Dividing and Main Caucasian Ranges to the north. 10% of the total population of the country lives in the North Caucasus.
2. Abkhazia also has territories that are parts of the Greater Caucasus: the area from the Kodori to the Gagra ranges, the Black Sea coast between the river. Psou and Enguri, and to the north of Enguri a small part of the Colchis lowland.
3. South Ossetia is located in the central region of the Greater Caucasus. The beginning of the territory is the Main Caucasian Range. The territory extends in a southerly direction from it, between the Rachinsky, Suramsky and Lomissky ranges, to the very valley of the Kura River.
4. Georgia has the most fertile and populated parts of the country in the valleys and lowlands between the Lesser and Greater Caucasus ranges to the west of the Kakheti range. The most mountainous parts of the country are Svaneti, a section of the Greater Caucasus between the Kodori and Suram ranges. The Georgian territory of the Lesser Caucasus is represented by the Meskheti, Samsar and Trialeti ranges. It turns out that the whole of Georgia is within the Caucasus.
5. Azerbaijan is located between the Dividing Range in the north and the Araks and Kura rivers in the south, and between the Lesser Caucasus and the Kakheti Range and the Caspian Sea. And almost all of Azerbaijan (the Mugan Plain and the Talysh Mountains belong to the Iranian Highlands) is located in the Caucasus.
6. Armenia has part of the territory of the Lesser Caucasus (slightly east of the Akhuryan River, which is a tributary of the Araks).
7. Turkey occupies the southwestern section of the Lesser Caucasus, representing 4 eastern provinces of this country: Ardahan, Kars, partly Erzurum and Artvin.

The mountains of the Caucasus are both beautiful and dangerous. According to the assumptions of some scientists, there is a possibility that in the next hundred years the volcano (Mount Elbrus) may wake up. And this is fraught with catastrophic consequences for neighboring regions (Karachay-Cherkessia and Kabardino-Balkaria).

But, whatever it may be, the conclusion follows that there is nothing more beautiful than the mountains. It is impossible to describe all the magnificent nature of this fabulous mountain country. To feel it all, you should visit these amazingly beautiful paradise places. They are especially impressively viewed from the heights of the peaks of the Caucasus Mountains.